Related Experiment Video
Updated: Feb 11, 2026

Utilizing Soil Density Fractionation to Separate Distinct Soil Carbon Pools
Published on: December 16, 2022
[Carbon sequestration in soil particle-sized fractions during reversion of desertification at Mu Us Sand land.]
Jian Ye Ma1, Xiao Gang Tong2, Zhan Bin Li3
1Institute of Soil and Water Conservation, Northwest A&F University/State Key Laboratory of Soil Erosion and Dry Land Farming on the Loess Plateau, Yangling 712100, Shaanxi, China.
Abstract:
The aim of this study was to investigate the effects of carbon sequestration in soil particle-sized fractions during reversion of desertification at Mu Us Sand Land, soil samples were collected from quicksand land, semifixed sand and fixed sand lands that were established by the shrub for 20-55 year-old and the arbor for 20-50 year-old at sand control region of Yulin in Northern Shaanxi Province. The dynamics and sequestration rate of soil organic carbon (SOC) associated with sand, silt and clay were measured by physical fractionation method. The results indicated that, compared with quicksand area, the carbon content in total SOC and all soil particle-sized fractions at bothsand-fixing sand forest lands showed a significant increasing trend, and the maximum carbon content was observed in the top layer of soils. From quicksand to fixed sand land with 55-year-old shrub and 50-year-old arbor, the annual sequestration rate of carbon stock in 0-5 cm soil depth was same in silt by 0.05 Mg·hm-2·a-1. The increase rate of carbon sequestration in sand was 0.05 and 0.08 Mg·hm-2·a-1, and in clay was 0.02 and 0.03 Mg·hm-2·a-1 at shrubs and arbors land, respectively. The increase rate of carbon sequestration in 0-20 cm soil layer for all the soil particles was averagely 2.1 times as that of 0-5 cm. At the annual increase rate of carbon, the stock of carbon in sand, silt and clay at the two fixed sand lands were increased by 6.7, 18.1 and 4.4 times after 50-55 year-old reversion of quicksand land to fixed sand. In addition, the average percentages that contributed to accumulation of total SOC by different particles in 0-20 cm soil were in the order of silt carbon (39.7%)≈sand carbon (34.6%) > clay carbon (25.6%). Generally, the soil particle-sized fractions had great carbon sequestration potential during reversion of desertification in Mu Us Sand Land, and the slit and sand were the main fractions for carbon sequestration at both fixed sand lands.
More Related Videos
Related Concept Videos
The Colonization of Land
Basic Postulates of Kinetic Molecular Theory: Particle Size, Energy, and Collision
The Carbon Cycle
The Soil Ecosystem
Precipitate Formation and Particle Size Control
The obtained precipitate should be either a pure substance of known composition or easily converted to one by a simple process, such as ignition or drying. In addition, the precipitate should be insoluble and easily filterable. In general, filterability...
Factors Affecting Dissolution: Particle Size and Effective Surface Area

